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Pocaterra Creek Member

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Stratigraphic columns of Pocaterra Creek Member (PCM) of the Cadomin Formation. Column on the left is of the PCM type section on Pocaterra Ridge (modified from Ricketts and Sweet 1986, fig. 19). The palynomorph assemblage analyzed by Ricketts and Sweet (1986) was collected approximately 41 m above the base of the PCM. Column on the right is the section we measured on Grizzly/Highwood Ridges, where the vertebrate fossil specimens UALVP 59792–UALVP 59794 were found. The “needle” siltstone is characteristic of the upper third of the Elk Formation (Ricketts and Sweet 1986). Sediment grain size abbreviations: c, clay; p, pebble; s, sand; and z, silt.
Published: 19 December 2019
Fig. 2. Stratigraphic columns of Pocaterra Creek Member (PCM) of the Cadomin Formation. Column on the left is of the PCM type section on Pocaterra Ridge (modified from Ricketts and Sweet 1986 , fig. 19). The palynomorph assemblage analyzed by Ricketts and Sweet (1986) was collected
Journal Article
Published: 01 September 1999
Bulletin of Canadian Petroleum Geology (1999) 47 (3): 199–222.
.... The Pocaterra Creek Member is a conglomerate, mudstone, and caliche-bearing subunit of the Cadomin Formation, having a restricted westerly distribution. The ages of the Cadomin and Dalhousie formations have not been well constrained previously because the units are generally too coarse-grained for optimum...
Journal Article
Published: 01 March 1997
Bulletin of Canadian Petroleum Geology (1997) 45 (1): 1–24.
...Dale A. Leckie; R.J. Cheel ABSTRACT The Lower Cretaceous Cadomin Formation has been traditionally subdivided into the Pocaterra Creek Member and overlying undifferentiated Cadomin. The Cadomin Formation in southwestern Alberta is a relatively thin, aerially extensive, sheet of conglomerate...
Journal Article
Published: 01 March 1986
Bulletin of Canadian Petroleum Geology (1986) 34 (1): 1–16.
... Cordillera: the Pocaterra Creek Member (Columbian Orogeny of southern Alberta), the Summit Creek Formation (Laramide Orogeny of Fort Norman area), and the Monster Formation (probably Laramide Orogeny of west-central Yukon) show a remarkable similarity in lithofacies despite large temporal and spatial...
Journal Article
Published: 19 December 2019
Canadian Journal of Earth Sciences (2020) 57 (4): 542–552.
...Fig. 2. Stratigraphic columns of Pocaterra Creek Member (PCM) of the Cadomin Formation. Column on the left is of the PCM type section on Pocaterra Ridge (modified from Ricketts and Sweet 1986 , fig. 19). The palynomorph assemblage analyzed by Ricketts and Sweet (1986) was collected...
FIGURES | View All (7)
Journal Article
Published: 01 June 1979
Bulletin of Canadian Petroleum Geology (1979) 27 (2): 183–208.
..., the Elk is possibly conformably overlain by the Pocaterra Creek Member of the Cadomin Formation (Blairmore Group). The Kootenay Group grades laterally into strata of the Nikanassin Formation in the vicinity of the North Saskatchewan River. 1 Geological Survey of Canada, Institute of Sedimentary...
Image
Geographic and stratigraphic position of vertebrate fossils described in this study (UALVP 59792–UALVP 59794), indicated by star. (A) locality within southwestern Alberta; (B) close-up of study area, with colour-coded Upper Jurassic and Lower Cretaceous units mapped on (McMechan 1998, 2013); (C) stratigraphic column of units in Fig. 1B, as exposed in southwestern Alberta (modified from White and Leckie 1999, fig. 2); (D) photograph of study area (facing southeast, taken from Pocaterra Creek Member type section area), with contacts between units (dotted lines) based on McMechan (1998, 2013); (E) photograph of partial osteoderm of an ankylosaurian in matrix; and (F) photograph of helicopter airlifting fossil-bearing sandstone blocks from site. The exposure of the Cadomin Formation (orange and red) in Fig. 1B that lies northwest of the fossil locality represents the type section of the Pocaterra Creek Member (Allan and Carr 1947). The yellow-coloured rocks in Fig. 1B represent Quaternary deposits. Map in Fig. 1A created with Adobe Illustrator CS5.1. Map in Fig. 1B created with Adobe Illustrator CS5.1. [Colour online.]
Published: 19 December 2019
, 2013 ); (C) stratigraphic column of units in Fig. 1B , as exposed in southwestern Alberta (modified from White and Leckie 1999 , fig. 2); (D) photograph of study area (facing southeast, taken from Pocaterra Creek Member type section area), with contacts between units (dotted lines) based on McMechan
Journal Article
Published: 01 August 1977
Bulletin of Canadian Petroleum Geology (1977) 25 (4): 767–791.
... and conglomerate of the Pocaterra Creek Member of the Blairmore Group (Allan and Carr, 1947). NOMENCLATURE Since first recognized and named by Dawson (1886), Kootenay rocks have been studied in two main areas: the region east of Lewis Thrust Fault (for location, see Price, 1962), including the economically...
Journal Article
Journal: AAPG Bulletin
Published: 01 March 1959
AAPG Bulletin (1959) 43 (3): 590–640.
... defined in the electric log. The Pocaterra Creek member, named by Allan and Carr (1947), was observed only in the Highwood area. On Picklejar Creek in Sec. 6, T. 18, R. 6, W.5th Mer., the member is 74.5 feet thick. The base of the Pocaterra Creek member is marked by a 21-foot bed of chert-pebble...
FIGURES | View All (24)
Journal Article
Published: 01 August 1977
Bulletin of Canadian Petroleum Geology (1977) 25 (4): 792–827.
... Alberta and southeastern British Columbia, a unit of mixed conglomerate, sandstone and mudstone with Blairmore affinities has been noted below the actual Cadomin conglomerate, and was named the Pocaterra Creek Member (Allan and Carr, 1947). Gibson (1977a,b) suggested that in western sections this unit may...